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Keli Highland
The Keli (Qeli) Highland ( ka, ყელის ზეგანი, ''qelis zegani'') is a volcanic field in Georgia on the western side of the Jvari Pass south to the Greater Caucasus range. More than thirty volcanic edifices on an area of 20x30km2 make up this volcanic field, which consists mostly of monogenetic volcanic structures. The lavas are rhyolites, trachyandesites and andesites. The rivers Tetri Aragvi, Patara Liakhvi, Ksani and Didi Liakhvi originate from the Keli volcanic area, and some peaks drain into the Terek river. Several mountain ranges separate the area into distinct high plains. Quaternary Dacite lava flows overlie thich Mesozoic sedimentary sequences. Western Khorisar (elevation 3736 m) and Didi-Nepiskalo (3694 m) are the highest summits close to the crest of the Greater Caucasus. In the northeastern part of the system are the Nepiskalo volcanoes and several smaller structures. The Patara-Nepiskalo volcano is strongly degraded by glacial action and may ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keli Lake
Keli Lake ( ka, ყელის ტბა; os, Хъелы цад, ''Qely cad'') is a volcanic-glacial lake in the Akhalgori Municipality, Mtskheta-Mtianeti region of Georgia. Located in Caucasus Mountains, in Keli Highland, at 2914 m above sea level. Stuck between Kharuli and Alevi ranges. The area of surface is 1.28 km², while the catchment area is 7.8 km². Average depth is 24,7 m, maximal depth is 63 m. Gets its feed from snow, rainfall and underground waters. River Ksani outflows from the Lake. Its water is clear.Georgian Soviet Encyclopedia The ''Georgian Soviet Encyclopedia'' ( ka, ქართული საბჭოთა ენციკლოპედია, ქსე) is the first universal encyclopedia in the Georgian language, printed in Tbilisi from 1965, the editor in chi ..., Ilia Apkhazava, V. 11, pp. 633-634, 1987. References {{Lakes of Georgia Lakes of Georgia (country) Lakes of South Ossetia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greater Liakhvi River
The Great Liakhvi ( ''Didi Liakhvi'', , ''Styr Lewakhi'') is a river in central Georgia, which rises on the southern slopes of the Greater Caucasus Mountain Range in the de facto independent region of South Ossetia and flows into the Kura (Mtkvari). It is long, and has a drainage basin of . The cities of Tskhinvali
Tskhinvali ( ka, ცხინვალი ) or Tskhinval ( os, Цхинвал, Чъреба, Tskhinval, Chreba, ; rus, Цхинва́л(и), r=Tskhinvál(i), ) is the capital of the dispute ...
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Volcanic Fields
A volcanic field is an area of Earth's crust that is prone to localized volcanic activity. The type and number of volcanoes required to be called a "field" is not well-defined. Volcanic fields usually consist of clusters of up to 100 volcanoes such as cinder cones. Lava flows may also occur. They may occur as a monogenetic volcanic field or a polygenetic volcanic field. Description Alexander von Humboldt observed in 1823 that geologically young volcanoes are not distributed uniformly across the Earth's surface, but tend to be clustered into specific regions. Young volcanoes are rarely found within cratons, but are characteristic of subduction zones, rift zones, or in ocean basins. Intraplate volcanoes are clustered along hotspot traces. Within regions of volcanic activity, volcanic fields are clusters of volcanoes that share a common magma source. Scoria cones are particularly prone to cluster into volcanic fields, which are typically in diameter and consist of several tens ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Georgia (country)
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
